Rising Temperatures Extend Community Size-Structure Damage Done by Decades of Size-Selective Fishing

Results from a Size Spectrum Analysis of the Northeast US Groundfish Community

Author

Affiliation

Adam A. Kemberling

Gulf of Maine Research Institute

Potential Journals:

1. Global Change Biology
2. ICES Journal of Marine Science

Abstract

The Northwest Atlantic ocean bordering the United states and Nova Scotia is one of the fastest warming locations on Earth. Research on the impacts of this rapid-warming has primarily focused on high-profile and/or upper trophic level species. Here we investigate an the ecosystem wide impacts by integrating community size structure changes using size spectrum analysis. While laboratory studies and ecological theory suggest that ectotherms raised at higher temperatures will reach smaller body-sizes at comparable development stages, it is unclear whether that relationship can be mitigated against through the adaptive behaviors of diverse communities. In cases where community responses fail at adapting to elevated temperatures, we anticipate a steepening of the body-size spectrum slope relating to a reduction in larger sized individuals and an increase in smaller sized individuals within that community. Using data from fisheries independent surveys we estimated size spectrum indices for four regions along the US NE continental shelf. At this regional scale, we found that declines in the size spectrum slopes occurred the strongest in the Northernmost regions of the Gulf of Maine and Georges Bank. These areas were historically home to the coldest temperatures and the largest populations of commercially targeted groundfish species. Size spectrum slope declines were more pronounced in the 80’s and 90’s, before to the more-recent elevated temperatures. This suggests that other external forces likely drove the initial declines of larger-sized individuals within the communities. While the primary pressure of fisheries exploitation has declined over time, the recovery of larger-sized individuals has not been seen and remains threatened by elevated temperatures.

Introduction

Temperature & Ecology

It is well understood that temperature plays a critical role on physiology through its impact on the chemical reactions that underpin biological life. A consequence of this, is that most life has evolved a thermal preference, around which the chemical reactions that support things like growth and means for self-preservation. Species that are unable to maintain their optimal thermal preferences internally (ectotherms), must be able to follow their thermal preferences through locomotion or adapt through changes in behavior. Otherwise; there will be physiological and/or metabolic costs in failing to do so.

In an era of anthropogenic climate change, there is an expectation that many species will be displaced from historic habitats. Research in marine environments has shown examples of species shifting to higher latitudes and deeper depths in the pursuit of more favorable conditions (Kleisner et al. 2017; Pinsky et al. 2013). Other research has suggested that the impacts of elevated temperatures may be manifesting not through geographic distribution change, but through physiological changes, changes in seasonal phenology, or hampered recovery efforts (Daan et al. 2005; Miller, O’Brien, and Fratantoni 2018; A. Pershing et al. 2018; University of South Carolina et al. 2021). Temperature has direct and indirect impacts on critical biological functions including the acquisition of biomass through feeding, the rates of biomass loss through metabolism, and the rates at which individuals mature and develop. This potential for temperature to impact the size structure of an ecosystem has implications for blue economy & natural resource systems we rely upon.

Size Spectrum Theory

Size is a defining characteristic of species that mediates many ecological interactions (Brown, West, and Enquist 2000). Size impacts the mobility of an organism, its ability to evade predation, its ability to successfully prey on other organisms, and the metabolic costs associated with each of these behaviors. In the context of a strongly size-structured ecosystem, growth and maturity changes alter fitness and ultimately determine whether a species is successful in the given environment. Size structured environments are a fundamental organizational pattern that has been heavily researched. Ecological theory is rich with models relating how energy transfers from smaller prey species to larger predatory trophic levels, the allocation of energy for growth, and the trade offs of allocating energy towards reproduction at the expense of growth. One such ecological model that avoids the need for explicit articulation of each predator-prey interaction is the size spectrum model.

A “size spectrum” describes the distribution of biomass or abundance as a function of individuals’ mass or size on a log–log scale (Guiet, Poggiale, and Maury 2016). Size spectrum are described by two terms, the size spectrum slope & intercept. These two terms convey the baseline productivity, and how energy flows through an ecosystem in the form of biomass. The spectrum intercept value captures the richness or the productivity at the base of the community and is strongly connected to the prevailing environmental conditions (Boudreau and Dickie 1992). So much so, that spectrum shape is sometimes defined by its eutrophic or oligotrophic environmental conditions (Rossberg 2012).

Size spectra condense the complexities of predator prey networks and their interactions into a handful of size-based indices (SBI). In doing so a community size spectrum captures the emergent properties of a system, while needing only size and abundance information that is commonly available. For this reason it has become increasingly relied upon as an indicator of ecosystem health in the push for ecosystem based fisheries management. Changes in slope have been associated with fishing exploitation, primarily through the targeted removal of larger individuals (Bianchi et al. 2000; Shin et al. 2005). Numerical experiments have also tried to link changes in slope to environmental disturbances (Guiet, Poggiale, and Maury 2016). Biomass spectrum present predictable intercepts between ecosystems of similar productivity levels, but also of distinct temperatures (Guiet, Poggiale, and Maury 2016).

This is a direct quote from (Guiet, Poggiale, and Maury 2016), but nails the connection back to temp expectations:

Because it controls chemical reactions, temperature controls metabolic rates which underpin maintenance, growth or reproduction (Clarke and Johnston, 1999; Kooijman, 2010) as well as the functional responses to food density (Rall et al., 2012). Guiet et al. (2016)… In addition to the impact of temperature on communities’ intercepts (heights), the impact of temperature on the speed of the energy flow within communities may affect other properties, such as their resilience to perturbations or the intensity of trophic cascades (Andersen and Pedersen, 2009).

Temperature of the Gulf of Maine & NE Shelf

• Marine species distribution shifts in NE Atlantic shelf (Kleisner et al. 2017)

Sea surface temperatures in the Gulf of Maine since 1982 have been warming at rates faster than 96% of the world’s oceans, with similar warming rates along the northwest Atlantic shelf (A. Pershing et al. 2018). A punctuated elevation in temperatures over the last decade are believed to be the result of a shift in Gulf Stream positioning. A Northward shift in the Gulf stream has increased the regional temperatures via an increased direct transport of warm gulf stream water into areas like the Gulf of Maine . The Gulf stream has also been producing a higher frequency of warm core rings, and has obstructed some of the cold-water Scotian Shelf current flow that would otherwise counter the influence of the Gulf Stream on the region’s temperatures (Gangopadhyay et al. 2019; University of South Carolina et al. 2021). The combination of these oceanographic changes has led to a warmer continental shelf habitat.

Species Trends in NE Shelf

The continental shelf groundfish community in Northwest Atlantic has changed dramatically over the last century. Stocks that supported international fishing effort collapsed, and recovery efforts fell short of their objectives. Research on Georges Bank estimated that biomass more than halved in the 1960’s (pre-dating federal monitoring efforts), and noted a species replacement of commercial groundfish target species by skate and dogfish (Fogarty and Murawski 1998). Fishing is inherently size-selective, with larger individuals selectively removed from the population. This has an immediate impact on the community size-distribution with additional impacts on the future population as well. Larger individuals have a greater impact on population recovery, capable of holding more (and often of higher quality) eggs. Size-based harvest in fisheries has been shown to create selective pressures that promote characteristics of early maturation at smaller sizes.

In addition to the ecological disturbance of fisheries removals, this region is also one of the fastest warming locations in the global oceans. The rapid warming in the northwest Atlantic is a major factor in the redistribution of marine species along the US east coast. Species have responded by adjusting the timing and locations of their seasonal migrations and shifting their geographic ranges (Nye et al. 2009; Staudinger et al. 2019). There is evidence that warming has hampered fisheries recoveries as well. Adding a metabolic tax to physiological pathways like growth and metabolism. Species like Black Sea Bass, Atlantic shortfin squid, and Blue crab have been high-profile examples of species expanding their ranges to follow their thermal preferences. While species like the American lobster have shown declines at their southern range near Long Island Sound, with much doubt whether they will recover under the present temperature trends. The recent regime shift in the physical oceanography has also shown to be a catalyst for biological shifts as well (University of South Carolina et al. 2021; Perretti et al. 2017).

While these examples show that species can respond to changes in the physical environment around them through movement & behavior, research elsewhere suggests that physiological responses integrated across species will manifest as changes in community size structure.

Purpose

With the understanding that populations depend on the health of their ecosystems, there is a need to have community-wide metrics to effectively understand and manage marine resources. Size based indices are metrics that can be estimated from the information that has historically been available from long-term survey efforts. These indices have been shown to be sensitive to the impacts of fishing, but should also capture environmentally driven stress as well. In this way they have the potential to track ecosystem wide signals of community health that are otherwise overlooked when looking through a single-species recovery lens, and might overlook factors beyond life-history traits like environmental disturbances like warming. Warming alters the community through the direct influence of temperature on metabolism, growth, and population productivity. In the case of the NW Atlantic, we anticipate that sustained increases in temperature should have an impact on the community size structure for the region that can be detected through the community biomass size spectra parameters. To this goal, we estimated size spectrum relationships as SBI’s for the groundfish populations for each sub-region of the Northeast US continental shelf.

Methods

Groundfish Data

Fishery Independent data on was collected as part of the NEFSC’s northeast trawl survey. This survey is conducted each year in the spring and in the fall, with sample locations determined following a stratified-random survey design with effort allocated in proportion to stratum area. Trawls are performed for a fixed duration at each station, reporting abundance at length and total biomass for all species caught. Trawl survey analyses incorporated data from both the Spring and Fall survey seasons, and for all years from 1970 to 2019. Correction factors were applied to total species abundance and aggregate species biomass to account for all changes in vessels, gear, and doors when appropriate as part of the survey program. However, abundance and biomass at length is not corrected for as part of the standard survey data protocol and needed to be estimated. To account for this, abundance at length for each species were adjusted to match the correction factors applied to total species abundance at each station, with allocations following the distributions of length caught at that station. Such that for each species: the sum of the resulting adjusted abundance numbers across each length is equal to the total abundance that was corrected for changes in vessels, gear, etc. To account for differences in sampling effort among survey strata, all corrected abundance-at-length data was then area-stratified.

Data from the survey was grouped by strata to form geographically meaningful sub-regions: Gulf of Maine, Georges Bank, Southern New England, Mid-Atlantic Bight. For each region, we developed several time series indicators:

1. Community Composition metrics (abundance and biomass by functional group, with body-size contributions)

2. Mean size of the aggregate community and key functional groups

3. Slope and intercept of the size spectrum

Community Composition

Functional groups were assigned to each species based on life history and geography. Functional groups included were elasmobranch, pelagic, demersal, and groundfish species. Stratified annual abundance and biomass totals were calculated for each functional group and each region with labels for increasing body-size (biomass kg) groups.

Body Size Trends

The annual stratified-abundance weighted body length and body weight within each region and for each functional group were also estimated using the numbers at length and the estimated biomass at length information. Data for body size trends was not truncated at 1g minimum body weight and is has not been adjusted to reflect any area-stratified estimation of abundance.

Size Spectrum Analysis

Community size spectra were estimated using abundance-at-length data from 68 species. These species were selected based on the availability of published weight-at-length relationships (Wigley et al. 2003) and represented 98.98% of the total biomass caught in the survey. Published length-weight relationships were used to convert abundance at length data into their corresponding biomass at length (kg). These values were then used to get totals for stratified weight-at-length, in complement to the corrected abundances-at-length data which had been area stratified. These area-stratified biomass at length totals were then used for fitting each regional biomass size spectra.

To fit the normalized biomass size spectra, stratified biomass at length data was binned into logarithmically equal spaced intervals (0.5 on a \(log_{10}\) scale), summing bodymass across all species within each body size bin. To normalize the spectra, the atratified abundances within each bin was then divided by the bin-width to account for the increasing bin-widths, a consequence of the log scale. Normalized size spectra were fit for each year and for each region independently, and for each year across all strata, using ordinary least squares (ols) regressions for stratified abundance (normalized) by body-size bins.

Temperature Data

Global Sea surface temperature data was obtained via NOAA’s optimally interpolated SST analysis (OISSTv2), providing daily temperature values at a 0.25° latitude x 0.25° longitude resolution (Reynolds et al. 2007). A daily climatology for every 0.25° pixel in the global data set was created using average daily temperatures spanning the period of 1982-2011. Daily anomalies were then computed as the difference between observed temperatures and the daily climatological average. OISSTv2 data used in these analyses were provided by the NOAA PSL, Boulder, Colorado, USA from their website at https://psl.noaa.gov.

Temperature data was regionally averaged to match the survey regions from the age-at-length data. SST anomalies were averaged by year for each region and over the entire sampling region to produce daily time series. These time series were then processed into annual timeseries of surface temperatures and anomalies. All region-averaging was done with area-weighting of the latitude/longitude grid cells to account for differences in cell-size in of the OISSTv2 data.

Spectra Drivers

The impact of external factors on the changes in size spectra was correlated against several hypothesized driving forces related to both environmental regimes and anthropogenic disturbances. Potential environmental drivers include sea surface temperature anomalies, Gulf Stream Index (GSI), and two zooplankton community indices derived from the Gulf of Maine continuous plankton recorder (CPR) program. Hypothesized anthropogenic drivers include state and federal fisheries landings from the Greater Atlantic Regional Fisheries Office (GARFO), divided by reporting zones into aggregate regions to closely align with the survey areas we defined for the size spectra analyses.

Results

Abundance Distribution

Abundance across all body sizes remained relatively stable from the 1970’s before rising in the northern regions around 1990 beginning in the Gulf of Maine. Around this time abundances increased through the mid 2010’s. Further south in Georges Bank, abundances remained flat until the 2010’s, when overall abundance roughly tripled, only to fall back to previous amounts by the end of the century. Southern New England saw a less dramatic rise and fall that began just before 2010, again falling back to earlier levels by the end of the century. The Mid Atlantic Bight had relatively consistent abundances throughout, with no major periods of abundance growth or decline, but with larger inter-annual variability.

Abundance gains observed in Georges Bank and Gulf of Maine were primarily from groundfish species, with additional growth from demersal species in the Gulf of Maine. Increases in abundance across all areas was mostly confined to individuals weighing less than .5kg. With some years driven in large-part by exceptional year-classes in a handful of species like haddock in Georges Bank. The observed abundance volatility in Southern New England and the Mid-Atlantic Bight conversely was largely the result of changes in abundance in pelagic species, whose abundance varied by several times the magnitude that of the other functional groups.

Biomass Distribution

Overall biomass was highest in the two northern regions, the Gulf of Maine and Georges Bank. Roughly half of the biomass sampled in these regions can be attributed to groundfish/demersal species, with the second largest contributions coming from elasmobranchs. Groundfish biomass, larger individuals >2kg in particular, declined during the 70’s and 80’s in these regions, never truly recovering. Beginning in the 2000’s there were signs that groundfish abundances were increasing as evidenced by increasing numbers of smaller individuals, however in both regions this trend appears to have reversed by the mid 2010’s. Elasmobranch biomass increased steadily throughout the survey time period across all regions, with the exception of southern New England. This area showed large 5-10 year swings in biomass, but no clear long-term trend. Larger elasmobranch were rare in all regions except for a period spanning the late 70’s through the early 90’s isolated to Georges Bank. Demersal species biomass was highest in the Gulf of Maine, dwarfing their contributions in other regions. Their biomass declined in the 70’s, was flat until the late 90’s, remaining relatively high until declining in the late 2010’s. Pelagic species biomass was low in all regions, and is unlikely to be representative of true biomass trends due to gear selectivity.

Regional Variation in Species Composition

There was a distinct difference between Northern and Southern regions in the way biomass was distributed among the different functional groups. The primary contributors to overall biomass in the southern regions (southern New England & mid-Atlantic bight) was the elasmobranch community. While the northern regions (Gulf of Maine & Georges Bank) each had similar quantities of elasmobranch biomasses, there was also a comparable contribution of groundfish and in the Gulf of Maine there was a major component of demersal species as well.

Body Size Trends

The average fish size in the Gulf of Maine (length and weight) declined the greatest of all regions over our study period. The average individual length was greatest in the 1970’s in the 35-40cm range, falling to 28-33cm over the last decade. Body-weight fell dramatically in the 1980’s, from around .75kg in the 1970’s to .25-.30kg, roughly a third of what it had been. Georges Bank body sizes also declined during the study period, but less dramatically. Both of these Northern regions had brief period in the late 2000’s where average length and weight rose, before falling again in the 2010’s. The MAB region was the only region to see a long-term increase in both length and weight during the study period. SNE saw no long-term change in length, and a minor decline in average body-weight.

All Species

Functional Group Length

Functional Group Bodymass

Regional Size Spectra

Beginning in the 1970’s, there was a clear difference in the relative positions of spectra parameters among the different regions. Gulf of Maine and Georges Bank showed the least steep spectra slopes in the earlier time periods with slopes around -1 & -1.1 respectively. The relatively flat slopes in these regions both steepened over time, settling near -1.3 (GoM) and -1.5 (GB). Gulf of Maine experienced much of its decline during the 1980’s and 1990’s. There was a brief reversal in this trend during the 2000’s, but slopes continued to steepen by 2010 and remained steep through 2019. Georges Bank did not experience as rapid of a decline, but experienced a similar long-term steepening. In contrast to the northern regions, SNE and MAB had steeper slopes in the -1.2 to -1.5 territory. The long term pattern for SNE was one of increasing volatility, but not so much a decline. The spectra slope for the MAB was less volatile, but similarly maintained a relatively stable wander around -1.4. By the end of the study period all regions had slopes that were at or near a similar level.

Size Spectra Drivers

Driver Correlations

Regime 1 (1970 - 2005)

Regime 2 (2006-2019)

Full Time Series

Discussion

• Top-down and bottom up influences on both carrying capacity (intercept) and transfer efficiency (slope)

Some of the major drivers suggested here operate on both, but to varying degrees. Here are some potential mechanisms:

Literature suggests: - Intercept (a proxy for productivity and carrying capacity) is primarily determined by bottom up features like: nutrient availability, temperature - Slope (a measure of energy transfer efficiency and static biomass distribution) has been shown to be sensitive to the physical removal of larger individuals.

Temperature Mechanisms: - Temperature’s impact on growth via genetic plasticity impacts both the available biomass at the primary producer level, as well as the Linf of larger species. - Temperature also impacts the efficiency of energy (as biomass) being transferred between individuals via predator & prey interactions. More energy per-capita is expended in the form of increased metabolic rates and/or behavioral changes. This metabolic tax should steepen the spectrum slope by removing available energy at a system wide level.

Separating Complimentary Forces Impacting Growth

The data we rely on in this analysis was collected as part of a survey program which began out of concern that fisheries were already being over-harvested. Estimates by scientists at that time suggested that by the 1970’s total biomass of Georges Bank had been halved and elasmobranchs had begun to replace the over-exploited gadoids (Fogarty and Murawski 1998). The implication of such a large disturbance that pre-dates our time series is that the steepening of size spectrum slope we observed in this area and the adjacent Gulf of Maine are the tail-ends of a longer and more severe decline. While metrics of overall fishing pressure is hard to align exactly with trawl survey coverage, historic and anecdotal evidence show that groundfish fishing pressures are a fraction of their historic pressure was in the 1960’s and 1970’s. This begs the question of why larger adult numbers never began to recover in these regions. Looking at abundance and biomass information from the survey there was evidence of strong recruitment among smaller individuals < 1kg, but there has since not been any sizable population of fishes larger than 1kg outside of elasmobranchs. Work by (A. J. Pershing et al. 2015) suggested that part of the failure in recovery was due to an inability to account for temperature change in fisheries management. At this point in time the regional temperatures had only begun to resemble a regime shift, and could have been considered at that time an acute stressor. Since that time the region has experienced nearly a decade of sustained above-average temperatures, and there are signs that the success seen in recruitment and survival of even the smaller size classes is declining. While temperature change has been associated with changes in growth rates and size-at-age, so too have size-selective fishing practices, making it difficult to disentangle the importance of exploitation & temperature on the overall community size structure when body size integrates these two forces (Shackell and Frank 2007).

Potential Drivers Timeseries:

Surface Temperature Anomalies

GARFO Landings

Climate Modes

CPR PCA

Determining Index Credibility

Our ability to make statements on community size-structure change in this study is limited by the community that is effectively sampled as part of the groundfish survey, and of species with available weight-at-length information. When looking at the composition of total biomass in each region separated out by species and by functional groups it became clear that in SNE and MAB a larger proportion of the community biomass was held within a relatively small number of species, primarily the elasmobranchs. Whether or not this is incomplete representation of the community due to the sampling gear, or an accurate representation of the entire community is unclear. In these two regions the biomass spectra information is largely that of the elasmobranch community. Whether or not this is a sufficient fraction of the broader community, what key community members are absent, and what the ecological implications of this are remain unclear.

Looking at both the level of noise in the body-size trends and the size spectra parameters, the Gulf of Maine and Georges Bank seem to have the clearest signals coming through. It is likely not coincidental that these two regions also have large proportions of their sampled biomass represented by groundfish and demersal species, functional groups that are best sampled by a bottom trawl survey. Looking specifically at these two regions only, we see two parallel trends of declining body size (length and weight) among the community as a whole. We also simultaneously see a steepening of the size spectra slope. Both of these trends are slightly more severe in the Gulf of Maine.

Supplemental Materials

Species Functional Groups

Functional Group Assignments and Regional Presence/Absence
Common Name	Gulf of Maine	Georges Bank	Southern New England	Mid-Atlantic Bight
Coastal
Atlantic Croaker	X		X	X
Atlantic Thread Herring			X	X
Blueback Herring	X	X	X	X
Bluefish	X	X	X	X
Butterfish	X	X	X	X
Northern Kingfish		X	X	X
Southern Kingfish				X
Spanish Mackerel				X
Spanish Sardine				X
Spot			X	X
Striped Bass	X	X	X	X
Weakfish		X	X	X
Elasmobranch
Atlantic Angel Shark				X
Atlantic Sharpnose Shark				X
Barndoor Skate	X	X	X	X
Bullnose Ray			X	X
Chain Dogfish		X	X	X
Clearnose Skate			X	X
Cownose Ray				X
Little Skate	X	X	X	X
Rosette Skate	X	X	X	X
Roughtail Stingray			X	X
Sand Tiger				X
Sandbar Shark			X	X
Smooth Butterfly Ray				X
Smooth Dogfish	X	X	X	X
Smooth Skate	X	X	X	X
Spiny Butterfly Ray				X
Spiny Dogfish	X	X	X	X
Thorny Skate	X	X	X	X
Winter Skate	X	X	X	X
Groundfish
Acadian Redfish	X	X	X	X
American Plaice	X	X	X	X
Atlantic Cod	X	X	X	X
Atlantic Halibut	X	X	X
Atlantic Wolffish	X	X	X
Cusk	X	X	X	X
Fawn Cusk-Eel	X	X	X	X
Fourspot Flounder	X	X	X	X
Goosefish	X	X	X	X
Haddock	X	X	X	X
Longhorn Sculpin	X	X	X	X
Northern Searobin	X	X	X	X
Ocean Pout	X	X	X	X
Offshore Hake	X	X	X	X
Pollock	X	X	X	X
Red Hake	X	X	X	X
Sea Raven	X	X	X	X
Silver Hake	X	X	X	X
Spotted Hake	X	X	X	X
Summer Flounder	X	X	X	X
White Hake	X	X	X	X
Windowpane Flounder	X	X	X	X
Winter Flounder	X	X	X	X
Witch Flounder	X	X	X	X
Yellowtail Flounder	X	X	X	X
Pelagic
Atlantic Herring	X	X	X	X
Atlantic Mackerel	X	X	X	X
Buckler Dory	X	X	X	X
Round Herring	X	X	X	X
Reef
Atlantic Spadefish				X
Black Sea Bass	X	X	X	X
Blackbelly Rosefish	X	X	X	X
Cunner	X	X	X	X
Greater Amberjack			X	X
Scup	X	X	X	X
NA
American Shad	X	X	X	X
Atlantic Sturgeon				X
Functional group assignments adapted from ________

GARFO Landings Summary

Largest Commercial Fisheries Landings of Northeastern US (by weight)
Harvest Region	Common Name	Avg. Annual Landings (lb.)	Total Landings (lb.)	Total Value ($)
1964 - 1995
Gulf of Maine	Herring, Atlantic	22.03M	1.89B	90.80M
Gulf of Maine	Menhaden, Atlantic	16.74M	954.35M	25.26M
Gulf of Maine	Hake, Silver	4.43M	566.87M	48.39M
Gulf of Maine	Cod, Atlantic	2.57M	545.39M	244.17M
Gulf of Maine	Pollock	1.91M	399.19M	107.17M
Georges Bank	Cod, Atlantic	7.67M	866.96M	411.09M
Georges Bank	Haddock	3.99M	450.77M	145.62M
Georges Bank	Flounder, Yellowtail	2.72M	307.27M	147.00M
Georges Bank	Hake, Silver	2.37M	246.08M	23.00M
Georges Bank	Flounder, Winter	1.99M	226.42M	156.36M
Southern New England	Other Fish, Bony	6.28M	627.79M	6.54M
Southern New England	Menhaden, Atlantic	6.47M	523.77M	19.26M
Southern New England	Flounder, Yellowtail	2.27M	516.96M	171.50M
Southern New England	Hake, Silver	1.88M	425.64M	98.62M
Southern New England	Flounder, Winter	1.13M	256.20M	97.99M
Mid-Atlantic Bight	Menhaden, Atlantic	74.13M	3.26B	154.62M
Mid-Atlantic Bight	Flounder, Summer	818.13K	115.36M	106.29M
Mid-Atlantic Bight	Mackerel, Atlantic	755.21K	79.30M	8.82M
Mid-Atlantic Bight	Scup	489.82K	57.80M	23.82M
Mid-Atlantic Bight	Weakfish/Sea Trout, Squeteague	446.27K	55.34M	23.15M
1996 - 2021
Gulf of Maine	Herring, Atlantic	12.26M	404.62M	24.36M
Gulf of Maine	Shark, Dogfish, Spiny	1.68M	68.84M	11.49M
Gulf of Maine	Cod, Atlantic	730.89K	65.05M	81.46M
Gulf of Maine	Monkfish/Angler/Goosefish	551.36K	49.62M	78.13M
Gulf of Maine	Pollock	593.95K	48.11M	38.27M
Georges Bank	Cod, Atlantic	2.24M	114.02M	133.29M
Georges Bank	Herring, Atlantic	4.24M	97.43M	6.54M
Georges Bank	Hake, Silver	1.43M	76.96M	32.48M
Georges Bank	Flounder, Winter	1.15M	60.01M	66.94M
Georges Bank	Haddock	1.06M	53.82M	70.62M
Southern New England	Mackerel, Atlantic	1.79M	191.14M	28.09M
Southern New England	Herring, Atlantic	2.23M	151.97M	10.92M
Southern New England	Hake, Silver	1.20M	142.41M	66.15M
Southern New England	Menhaden, Atlantic	2.26M	106.37M	8.48M
Southern New England	Skate, Nk	1.02M	101.88M	14.21M
Mid-Atlantic Bight	Menhaden, Atlantic	83.91M	6.63B	468.26M
Mid-Atlantic Bight	Croaker, Atlantic	1.81M	188.04M	82.10M
Mid-Atlantic Bight	Mackerel, Atlantic	1.73M	121.11M	14.99M
Mid-Atlantic Bight	Bass, Striped	1.30M	79.47M	173.06M
Mid-Atlantic Bight	Spot	835.86K	57.67M	41.54M
Landings data obtained from the Greater Atlantic Regional Fishing Office (GARFO)

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